富蕴克默孜巴依铜镍矿成矿地质特征及成因浅析  

Analysis on Genesis and Mineralization Characterisitc of Kemozibayi Cu-Ni deposit in Fuyun County,Xinjiang

作　　者：郭旭吉 潘祎 曹旋 

机构地区：[1]新疆维吾尔自治区有色地勘局706地质队,新疆阿勒泰836500

出　　处：《新疆地质》2013年第F12期96-100,共5页Xinjiang Geology

基　　金：新疆维吾尔自治区地质勘查基金（A12-3-XJ02）项目资助

摘　　要：克默孜巴依基性岩体成矿地质背景、地球物理特征、岩体特征、矿体特征和矿床成因，证明其为岩浆熔离型铜镍矿床。与喀拉通克铜镍矿床为同源同期形成的与基性-超基性岩有关的铜镍硫化物矿床。The Kemozibayi marie intrusion in Fuyun County, Xinjiang,is located in the northern Irtysh compressive zone.Cu-Ni mineralization is hosted by olivine-gabbro and gabbro.The Kemozibayi deposit is a magamtic segregation type Cu-Ni deposit based on metallogenic geological setting,geophysical characteristics,mineralized intrusion and miner- alization features, and formed homologously and synchronously with Kalatongke Cu-Ni deposit.

关 键 词：富蕴 克默孜巴依 铜镍硫化物矿床 额尔齐斯构造带 

分 类 号：P618.41[天文地球—矿床学] P618.63[天文地球—地质学]